利用修订的经典图表和成分数据分析(CoDa)进行地下水质量评估:沙特阿拉伯 Wadi Ranyah 案例研究

IF 3.7 3区 综合性期刊 Q1 MULTIDISCIPLINARY SCIENCES Journal of King Saud University - Science Pub Date : 2024-09-24 DOI:10.1016/j.jksus.2024.103463
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引用次数: 0

摘要

本研究旨在评估沙特阿拉伯 Wadi Ranyah 地区浅含水层地下水的状况和化学性质,使用的稳健统计方法(CoDA)考虑到了从 Wadi Ranyah 谷地采集的 45 个地下水样本的化学分析数据的独特性。对成分数据采用了居中对数变换(clr)方法和等距对数变换(ilr)图,以确定不同的水类型,并了解影响该地区地下水化学的水文地质化学过程。主成分分析和 K-均值聚类的结果显示存在三个地下水组别:(i) 第一组占据补给区,微量金属元素(钙、铅、锰、锌)、pH 值和 TDS 之间存在关系,表明火成岩和变质岩矿物的蚀变作用。(ii) 第二组是 Al-Hujrah 地区下游的特征,钙和硝酸盐之间的关系表明农业活动的影 响。(iii) 第三组位于 Ranyah 地区,显示了主要离子(Na+、SO42-、Mg2+、HCO3-、Cl-、K+)之间的关系,说明了水矿化受到硅酸盐风化和蒸发现象的影响。根据修改后的派珀图(ilr Piper),可确定两个水化学面。上游地区被划分为 Ca-HCO3- 型,而下游地区被划分为 Na-K-HCO3- 型。水质指数 (WQI) 计算值表明,所有 Wadi Ranyah 地下水样本的水质都很差(WQI > 300)。这是因为污染元素(铅、锰和钙)的浓度较高,尤其是铅的浓度较高,在 0.24 至 0.4 毫克/升之间,远高于世界卫生组织规定的饮用水限值(0.01 毫克/升)。首次在该研究区域应用 CoDA,对地下水水质机制进行了更详细、更可靠的评估,为地下水资源管理提供了建议,并确定了未来的研究需求。
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Groundwater quality assessment using revised classical diagrams and compositional data analysis (CoDa): Case study of Wadi Ranyah, Saudi Arabia
This research aims to assess the status and chemical properties of groundwater in the shallow aquifer of the Wadi Ranyah region, Saudi Arabia, using robust statistical methods (CoDA) that take into account the unique characteristics of chemical analysis data from forty-five (45) groundwater samples collected in the Wadi Ranyah valley. A centered logarithmic transformation (clr) approach and isometric logarithmic transformation (ilr) plots for compositional data were utilized to determine the different water types and to understand the hydrogeochemical processes influencing groundwater chemistry in the region. The results of principal component analysis and K-means clustering reveal the existence of three groundwater groupings: (i) The first group occupies the recharge region with a relationship between trace metal elements (F, Pb, Mn, Zn), pH, and TDS, indicating the effect of alteration of igneous and metamorphic rock minerals. (ii) The second group characterizes the downstream part of the Al-Hujrah area with a relationship between calcium and nitrates, indicating the influence of agricultural activities. (iii) The third group, located in the Ranyah area, shows a relationship between major ions (Na+, SO42−, Mg2+, HCO3, Cl, K+), which explains water mineralization influenced by silicate weathering and evaporation phenomena. According to the modified Piper diagram (ilr Piper), two hydrochemical facies are identified. The upstream region is categorized as Ca-HCO3 while the downstream region is classified as Na-K-HCO3. Calculated water quality index (WQI) values indicate that all Wadi Ranyah groundwater samples are of very poor quality (WQI > 300). This is due to higher concentrations of polluting elements (Pb, Mn and F), in particular the high lead concentrations which vary between 0.24 and 0.4 mg/L, and are well above the WHO limit (0.01 mg/L) for consumption of drinking water. The application of CoDA for the first time in the study region has provided a more detailed and reliable assessment of the mechanisms governing groundwater quality, permitting suggestions for the management of groundwater resources and defining future research needs.
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来源期刊
Journal of King Saud University - Science
Journal of King Saud University - Science Multidisciplinary-Multidisciplinary
CiteScore
7.20
自引率
2.60%
发文量
642
审稿时长
49 days
期刊介绍: Journal of King Saud University – Science is an official refereed publication of King Saud University and the publishing services is provided by Elsevier. It publishes peer-reviewed research articles in the fields of physics, astronomy, mathematics, statistics, chemistry, biochemistry, earth sciences, life and environmental sciences on the basis of scientific originality and interdisciplinary interest. It is devoted primarily to research papers but short communications, reviews and book reviews are also included. The editorial board and associated editors, composed of prominent scientists from around the world, are representative of the disciplines covered by the journal.
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